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Hem, S. R., Makovicky, E., Gervilla, F. (2001) Compositional trends in Fe, Co and Ni sulfarsenides and their crystal-chemical implications: Results from the Arroyo de La Cueva deposits, Ronda Peridotite, Southern Spain. The Canadian Mineralogist, 39 (3). 831-853 doi:10.2113/gscanmin.39.3.831

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Reference TypeJournal (article/letter/editorial)
TitleCompositional trends in Fe, Co and Ni sulfarsenides and their crystal-chemical implications: Results from the Arroyo de La Cueva deposits, Ronda Peridotite, Southern Spain
JournalThe Canadian Mineralogist
AuthorsHem, S. R.Author
Makovicky, E.Author
Gervilla, F.Author
Hem, S. R.Author
Makovicky, E.Author
Gervilla, F.Author
Year2001 (June 1)Volume39
Page(s)831-853Issue3
PublisherMineralogical Association of Canada
Download URLhttps://rruff.info/doclib/cm/vol39/CM39_831.pdf+
DOIdoi:10.2113/gscanmin.39.3.831Search in ResearchGate
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Classification
Not set		LoC
Not set
Mindat Ref. ID63504Long-form Identifiermindat:1:5:63504:0
GUID0
Full ReferenceHem, S. R., Makovicky, E., Gervilla, F. (2001) Compositional trends in Fe, Co and Ni sulfarsenides and their crystal-chemical implications: Results from the Arroyo de La Cueva deposits, Ronda Peridotite, Southern Spain. The Canadian Mineralogist, 39 (3). 831-853 doi:10.2113/gscanmin.39.3.831
Plain TextHem, S. R., Makovicky, E., Gervilla, F. (2001) Compositional trends in Fe, Co and Ni sulfarsenides and their crystal-chemical implications: Results from the Arroyo de La Cueva deposits, Ronda Peridotite, Southern Spain. The Canadian Mineralogist, 39 (3). 831-853 doi:10.2113/gscanmin.39.3.831
In(2001, June) The Canadian Mineralogist Vol. 39 (3) Mineralogical Association of Canada

Mineral Pages

MineralCitation Details
Alloclasite
Löllingite
Westerveldite

See Also

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Fanlo, I.; Subias, I.; Gervilla, F.; Paniagua, A.; Garcia, B. (2004) The composition of Co-Ni-Fe sulfarsenides, diarsenides and triarsenides from the San Juan de Plan deposit, central Pyrenees, Spain. The Canadian Mineralogist, 42 (4). 1221-1240 doi:10.2113/gscanmin.42.4.1221
Hem, S. R., Makovicky, E. (2004) The System Fe-Co-Ni-As-S. II. Phase Relations in the (Fe,Co,Ni)As1.5S0.5 Section at 650° and 500°C. The Canadian Mineralogist, 42 (1). 63-86 doi:10.2113/gscanmin.42.1.63
Hem, S. R., Makovicky, E. (2004) THE SYSTEM Fe-Co-Ni-As-S. I. PHASE RELATIONS IN THE (Fe,Co,Ni)As0.5S1.5 SECTION AT 650° AND 500°C. The Canadian Mineralogist, 42 (1). 43-62 doi:10.2113/gscanmin.42.1.43
Fanlo, I., Subias, I., Gervilla, F., Manuel, J. (2006) Textures and compositional variability in gersdorffite from the Crescencia Ni–(Co–U) showing, Central Pyrenees, Spain: primary deposition or re-equilibration?. The Canadian Mineralogist, 44 (6) 1513-1528 doi:10.2113/gscanmin.44.6.1513
PEREIRA, M. D., SHAW, D. M., ACOSTA, A. (2003) MOBILE TRACE ELEMENTS AND FLUID-DOMINATED PROCESSES IN THE RONDA PERIDOTITE, SOUTHERN SPAIN. The Canadian Mineralogist, 41 (3) 617-625 doi:10.2113/gscanmin.41.3.617
Foit, F. F.; Ulbricht, M. E. (2001) Compositional variation in mercurian tetrahedrite-tennantite from epithermal deposits of the Steens and Pueblo Mountains, Harney County, Oregon. The Canadian Mineralogist, 39 (3). 819-830 doi:10.2113/gscanmin.39.3.819
Makovicky, Emil, Balić-Žunić, Tonči, Topa, Dan (2001) The crystal structure of neyite, Ag2Cu6Pb25Bi26S68. The Canadian Mineralogist, 39 (5) 1365-1376 doi:10.2113/gscanmin.39.5.1365
Makovicky, E., Makovicky, M., Rose-Hansen, J. (2002) THE SYSTEM Fe Rh S AT 900  AND 500 C. The Canadian Mineralogist, 40 (2) 519-526 doi:10.2113/gscanmin.40.2.519
Berlepsch, P., Armbruster, T., Makovicky, E., Hejny, C., Topa, D., Graeser, S. (2001) The crystal structure of (001) twinned xilingolite, Pb3Bi2S6 from Mittal-Hohtenn, Valais, Switzerland. The Canadian Mineralogist, 39 (6) 1653-1663 doi:10.2113/gscanmin.39.6.1653
Majzlan, J., Makovicky, M., Makovicky, E., Rose-Hansen, J. (2002) THE SYSTEM Fe Pt S AT 1100 C. The Canadian Mineralogist, 40 (2) 509-517 doi:10.2113/gscanmin.40.2.509
Karup-Moller, S., Makovicky, E. (2002) THE SYSTEM Fe Os S AT 1180 , 1100  AND 900 C. The Canadian Mineralogist, 40 (2) 499-507 doi:10.2113/gscanmin.40.2.499
 
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